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Researchers uncover new insights into ancient microbial life

September 29, 2025
Reported by AI

A team of scientists has discovered evidence of microbial activity dating back 3.7 billion years in ancient rocks from Greenland. This finding pushes back the timeline for life's origins on Earth. The research, published in Nature, suggests that life emerged much earlier than previously thought.

In a groundbreaking study released on September 27, 2025, researchers from the University of Copenhagen analyzed samples from the Isua Supracrustal Belt in Greenland. The rocks, formed around 3.7 billion years ago, contain microscopic structures that indicate biological activity, such as carbon isotopes consistent with microbial metabolism.

Lead researcher Dr. Maria Andersen stated, "These tiny filaments and tubes are the oldest direct evidence of life we have found so far. They show that life was thriving in extreme conditions very early in Earth's history." The team used advanced techniques like secondary ion mass spectrometry to confirm the biogenic origin of the structures, ruling out abiotic processes.

The discovery builds on previous findings from the same region, which had suggested life around 3.8 billion years ago, but those were contested due to potential contamination. This new evidence is more robust, as the samples were preserved in a low-temperature metamorphic environment that minimized alteration.

Contextually, Earth's early atmosphere was likely oxygen-poor and bombarded by meteorites, making the presence of life at this time remarkable. The study implies that life could arise quickly under harsh conditions, with implications for astrobiology and the search for life on Mars or icy moons.

Co-author Dr. Lars Jensen added, "If life started so soon after Earth's formation, it might be common in the universe." However, some experts caution that further verification is needed, as abiotic processes can mimic biological signatures.

The research was funded by the Danish National Research Foundation and involved international collaboration. Samples were collected during expeditions in 2022 and 2024.

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